Pregled bibliografske jedinice broj: 129309
A new Late Jurassic megatracksite from northern Switzerland
A new Late Jurassic megatracksite from northern Switzerland // 1st symposium on european dinosaurs, Programme and Abstracts / Sachs, Sven ; Windolf, Raymund (ur.).
Düsseldorf, 2000. str. 19-20 (predavanje, međunarodna recenzija, sažetak, znanstveni)
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Naslov
A new Late Jurassic megatracksite from northern Switzerland
Autori
Meyer, Christian ; Mezga, Aleksandar
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
1st symposium on european dinosaurs, Programme and Abstracts
/ Sachs, Sven ; Windolf, Raymund - Düsseldorf, 2000, 19-20
Skup
First Symposium on European Dinosaurs
Mjesto i datum
Düsseldorf, Njemačka, 14.03.2000. - 18.03.2000
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
sauropod megatracksite; tidal flat environment; Upper Jurassic; nothern Switzerland
Sažetak
Since the first discovery of a megatracksite in the Late Jurassic (Late Kimmeridgian sensu gallico) in the Northern Jura mountains, numerous tracksites have come to light. Following the documentation of another large tracksite in the Jura mountains additional sites have demonstrated that those constitute altogether a second megatracksite. Stratigraphic correlations indicate a Mid Kimmeridgian age. The southern limit of the megatracksite reveals tracks on three distinct levels (Moutier) whereas the northern border (Glovelier) yields six different levels. Within these recurrent associations more than 3000 individual footprints have been ragistered. Two different morphotypes of dinosaurs are present. Among those are medium-sized to large sauropod (wide-gauge type) and large theropods. The tracklevels occur at the end of small-scale "shallowing-upward" cycles and are often found in barren micrites that show fenestrate fabric, birds-eye and stromatolites. Those observations indicate a deposition in a tidal flat environment. The recurrent association of sauropod and theropod footprints over a large area (150 km') is consistent with the Brontopodus-ichnofacies concept.
Izvorni jezik
Engleski